2021
DOI: 10.1002/rcm.9027
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Ion‐exchange resin and denitrification pretreatment for determining δ15N‐NH4+, δ15N‐NO3, and δ18O‐NO3 values

Abstract: Rationale There has never been a highly sensitive method for simultaneously measuring the δ15N and δ18O values of nitrate ions (NO3−) and the δ15N values of ammonium ions (NH4+) in particulate matter using denitrifying bacteria. In this study, we explored a method that combines use of an anion‐exchange resin and denitrifying bacteria to make such measurements. Methods The δ15N‐NH4+ values of samples obtained using the hypobromite and denitrifying bacteria method were measured by isotope ratio mass spectrometry… Show more

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Cited by 5 publications
(2 citation statements)
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References 52 publications
(63 reference statements)
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“…Nutrient concentrations of nitrite (NO 2 − ), nitrate (NO 3 − ) and phosphate (PO 4 3− ) in seawater were determined by a San ++ continuous flow analyzer (Skalar, The Netherlands), the detection limits of which were 0.1 μmol L −1 for both NO 2 − and NO 3 − , and 0.03 μmol L −1 for PO 4 3− . The chemical method for the measurement of δ 15 N‐NO 3 − and δ 18 O‐NO 3 − was used in this study, which was widely used to measure nitrogen and oxygen isotopes of nitrate in coastal water (Casciotti & Mcilvin, 2007; Chen, Bardhan, et al., 2021; Granger & Sigman, 2009; Kawashima et al., 2020; Mcilvin & Altabet, 2005; Wong et al., 2020; Ye et al., 2016), and also used in open sea with oligotrophic water (Casciotti & Mcilvin, 2007; Chen, Bardhan, et al., 2021; Ye et al., 2016). After nitrite was removed by adding sulfamic acid (Granger et al., 2008), isotopic analysis of dissolved NO 3 − was conducted following a chemical conversion method modified from Mcilvin and Altabet (2005).…”
Section: Methodsmentioning
confidence: 99%
“…Nutrient concentrations of nitrite (NO 2 − ), nitrate (NO 3 − ) and phosphate (PO 4 3− ) in seawater were determined by a San ++ continuous flow analyzer (Skalar, The Netherlands), the detection limits of which were 0.1 μmol L −1 for both NO 2 − and NO 3 − , and 0.03 μmol L −1 for PO 4 3− . The chemical method for the measurement of δ 15 N‐NO 3 − and δ 18 O‐NO 3 − was used in this study, which was widely used to measure nitrogen and oxygen isotopes of nitrate in coastal water (Casciotti & Mcilvin, 2007; Chen, Bardhan, et al., 2021; Granger & Sigman, 2009; Kawashima et al., 2020; Mcilvin & Altabet, 2005; Wong et al., 2020; Ye et al., 2016), and also used in open sea with oligotrophic water (Casciotti & Mcilvin, 2007; Chen, Bardhan, et al., 2021; Ye et al., 2016). After nitrite was removed by adding sulfamic acid (Granger et al., 2008), isotopic analysis of dissolved NO 3 − was conducted following a chemical conversion method modified from Mcilvin and Altabet (2005).…”
Section: Methodsmentioning
confidence: 99%
“…This conversion is based on NH + 4 oxidation to NO − 2 by a hypobromite solution, with NO − 2 then reduced to N 2 O by a sodium azide / acetic acid solution. This second method has been applied to aerosol samples (Kawashima et al, 2021) but has not yet been applied to ice core analyses, likely due to challenges related to the smaller NH + 4 concentrations in ice.…”
mentioning
confidence: 99%